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dc.contributor.authorReddy, Vishnu
dc.contributor.authorSanchez, Juan A.
dc.contributor.authorFurfaro, Roberto
dc.contributor.authorLe Corre, Lucille
dc.contributor.authorHardersen, Paul S.
dc.contributor.authorBottke, William F.
dc.contributor.authorBrozovic, Marina
dc.contributor.authorBinzel, Richard P
dc.contributor.authorBurbine, Thomas
dc.date.accessioned2018-08-28T12:58:53Z
dc.date.available2018-08-28T12:58:53Z
dc.date.issued2018-03
dc.identifier.issn1538-3881
dc.identifier.urihttp://hdl.handle.net/1721.1/117573
dc.description.abstractOn 2029 April 13, near-Earth asteroid (NEA) (99942) Apophis will pass at a distance of ∼6 Earth radii from Earth. This event will provide researchers with a unique opportunity to study the effects of tidal forces experienced by an asteroid during a close encounter with a terrestrial planet. Binzel et al. predicted that close flybys of terrestrial planets by NEAs would cause resurfacing of their regolith due to seismic shaking. In this work, we present the best pre-encounter near-infrared spectra of Apophis obtained so far. These new data were obtained during the 2013 apparition using the NASA Infrared Telescope Facility (IRTF). We found that our spectral data is consistent with previous observations by Binzel et al. but with a much higher signal-to-noise ratio. Spectral band parameters were extracted from the spectra and were used to determine the composition of the asteroid. Using a naïve Bayes classifier, we computed the likelihood of Apophis being an LL chondrite to be >99% based on mol% of Fa versus Fs. Using the same method, we estimated a probability of 89% for Apophis being an LL chondrite based on ol/(ol+px) and Fs. The results from the dynamical model indicate that the most likely source region for Apophis is the ν6resonance in the inner main belt. Data presented in this study (especially Band I depth) could serve as a baseline to verify seismic shaking during the 2029 encounter.en_US
dc.publisherAmerican Astronomical Societyen_US
dc.relation.isversionofhttp://dx.doi.org/10.3847/1538-3881/AAAA1Cen_US
dc.rightsArticle is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use.en_US
dc.sourceIOP Publishingen_US
dc.titleSurface Composition of (99942) Apophisen_US
dc.typeArticleen_US
dc.identifier.citationReddy, Vishnu, Juan A. Sanchez, Roberto Furfaro, Richard P. Binzel, Thomas H. Burbine, Lucille Le Corre, Paul S. Hardersen, William F. Bottke, and Marina Brozovic. “Surface Composition of (99942) Apophis.” The Astronomical Journal 155, no. 3 (March 5, 2018): 140.en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Aeronautics and Astronauticsen_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciencesen_US
dc.contributor.mitauthorBinzel, Richard P
dc.contributor.mitauthorBurbine, Thomas
dc.relation.journalThe Astronomical Journalen_US
dc.eprint.versionFinal published versionen_US
dc.type.urihttp://purl.org/eprint/type/JournalArticleen_US
eprint.statushttp://purl.org/eprint/status/PeerRevieweden_US
dc.date.updated2018-08-24T11:53:58Z
dspace.orderedauthorsReddy, Vishnu; Sanchez, Juan A.; Furfaro, Roberto; Binzel, Richard P.; Burbine, Thomas H.; Le Corre, Lucille; Hardersen, Paul S.; Bottke, William F.; Brozovic, Marinaen_US
dspace.embargo.termsNen_US
dc.identifier.orcidhttps://orcid.org/0000-0001-8889-8692
mit.licensePUBLISHER_POLICYen_US


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